Inclination, declination and the reversal angle of the ChRM for CON01-603-2

DOI

Selected intervals of down-core variations of normalised relative paleointensity, ChRM inclination and declination, and the reversal angle. (A) Core CON 01-603-2: numbers in the simplified lithological column indicate marine isotope stages (MIS), after Fig. 3. The paleomagnetic data show a geomagnetic excursion with a short, but full, reversal of the local field vector at the beginning of MIS 6. (B) Core VER 98-1-1: in this case, the excursion represented by a strong deviation of the reversal angle during a period of low intensity occurs in MIS 3 and corresponds to the Laschamp event. (C) Core VER 98-1-1: in this case, the excursion is also represented by a strong deviation of the reversal angle during a period of low intensity. Again this occurs in MIS 3 and corresponds to the Laschamp event.

Identifier
DOI https://doi.org/10.1594/GFZ.SDDB.1009
Related Identifier https://doi.org/10.1016/j.gloplacha.2004.09.016
Metadata Access http://doidb.wdc-terra.org/oaip/oai?verb=GetRecord&metadataPrefix=oai_datacite&identifier=oai:doidb.wdc-terra.org:210
Provenance
Creator Demory, Francois; Nowaczyk, Norbert; Witt, Annette; Oberhänsli, Hedi
Publisher Deutsches GeoForschungsZentrum GFZ
Publication Year 2006
OpenAccess true
Contact www.icdp-online.org/contact
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 330 Datapoints
Discipline Scientific drilling
Spatial Coverage (108.913W, 53.953S, 108.914E, 53.963N)